ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
贵州晴隆矿区K6煤层的元素地球化学特征
  
关键词:coal  bornite  volcanic ash  Late Permian  Qinglong Mine
基金项目:国家自然科学基金项目(编号:40133010)
作者单位E-mail
李大华 中国矿业大学资源与地球科学系北京100083
重庆煤田地质研究所重庆400042 
ldh@vip.163.com 
唐跃刚 中国矿业大学资源与地球科学系北京100083  
陈坤 重庆煤田地质研究所重庆400042  
邓涛 重庆煤田地质研究所重庆400042  
程方平 重庆煤田地质研究所重庆400042  
刘东 重庆煤田地质研究所重庆400042  
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摘要:
Geochemistry of the K6 Coal Seam in the Qinglong Mine, Guizhou Province
      Geochemical characteristics of the Late Permian K6 Coal seam in the Qinglong Mine of western Guizhou Province were studied by such methods as inductively-coupled plasma-mass spectroscopy, X-ray fluorescence spectrometry, scanning electron microscopy equipped with energy-dispersive X-ray, and sequential chemical extraction. The results reveal that, in addition to Cu, S, and Fe, bornite is the main carrier of Bi and Pb. The high content of Cr, Cu, F, U, and Zr is attributed to the special material of volcanic origin.
LI Da-hua,TANG Yue-hua,CHEN Kun,DENG Tao,CHENG Fang-ping,LIU Dong.2006.Geochemistry of the K6 Coal Seam in the Qinglong Mine, Guizhou Province[J].Acta Geoscientica Sinica,27(2):135-140.
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